The Monte delle Erbe Limestone, formally defined as an Early Oligocene formation of the Monte Baldo area, and considered laterally equivalent to the Acquenere Formation, is in fact of Late Eocene (Priabonian) age. It is therefore equivalent to the Nago Limestone and stratigraphically underlying the Early Oligocene succession which is constituted by a lower pelagic unit (Bolognano Marls) and an upper shallow-water terrigenous-carbonate sequence, the Acquenere Formation proper.
Emendamenti alla stratigrafia paleogenica del Monte Baldo (Alpi meridionali, Italia) / Bosellini, Francesca; V., Luciani; A., Russo; A., Sirotti. - In: BOLLETTINO DELLA SOCIETÀ PALEONTOLOGICA ITALIANA. - ISSN 0375-7633. - STAMPA. - 27:(1988), pp. 361-366.
Emendamenti alla stratigrafia paleogenica del Monte Baldo (Alpi meridionali, Italia)
BOSELLINI, Francesca;
1988
Abstract
The Monte delle Erbe Limestone, formally defined as an Early Oligocene formation of the Monte Baldo area, and considered laterally equivalent to the Acquenere Formation, is in fact of Late Eocene (Priabonian) age. It is therefore equivalent to the Nago Limestone and stratigraphically underlying the Early Oligocene succession which is constituted by a lower pelagic unit (Bolognano Marls) and an upper shallow-water terrigenous-carbonate sequence, the Acquenere Formation proper.
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